ライフサイエンスコーパス: deep sea

1 the bioluminescence spectrum present in the deep sea.

2 a model chemosynthesizing bacterium from the deep sea.

3 of carbon dioxide by 'pumping' carbon to the deep sea.

4 atial planning of competing interests in the deep sea.

5 C as POC "Particulate Organic Carbon" to the deep sea.

6 sh assemblages along a depth gradient in the deep sea.

7 ter, to near shore to the open ocean and the deep sea.

8 ansfer of carbon from the upper ocean to the deep sea.

9 he dominating oligotrophic microbiota of the deep sea.

10 ndustrial activities now taking place in the deep sea.

11 to survive in the extreme conditions of the deep sea.

12 g to the challenges of observing them in the deep sea.

13 oil and gas remained in, or returned to, the deep sea.

14 yorkensis, a newly isolated microbe from the deep sea.

15 ganic carbon, and pollutant transport to the deep sea.

16 secluded and stable environment such as the deep sea.

17 ood bioindicator for MP contamination of the deep sea.

18 e water column and animal communities of the deep sea.

19 ant ecological trait from the surface to the deep-sea.

20 systems and are unusually energy rich in the deep-sea.

21 rthquakes on long-term carbon cycling in the deep-sea.

22 Deltaproteobacteria, three deep-sea clades (Deep sea-1/symbiont-like, Deep sea-2/PS-80 and Deep sea-

23 oth patterns and environmental predictors of deep-sea (2,000-6,500 m) species richness fundamentally

24 e deep-sea clades (Deep sea-1/symbiont-like, Deep sea-2/PS-80 and Deep sea-3/OPU3) within gammaproteo

25 ep sea-1/symbiont-like, Deep sea-2/PS-80 and Deep sea-3/OPU3) within gammaproteobacterial methanotrop

26 he cycling of carbon between the surface and deep sea(4,5).

27 ter column processes, particles reaching the deep sea (4000 m) are energy-replete with organic carbon

28 etectable against the dark background of the deep sea [5].

29 esting that the Antarctic and Southern Ocean deep-sea accumulates higher numbers of microplastic poll

30 Here, the response of the deep-sea aerobic methanotroph Methyloprofundus sedimenti

31 d high hydrostatic pressure prevalent in the deep sea affect toxicity, and whether adaptation to deep

32 After 170 y of deep sea aging in close-to-perfect conditions, these sle

33 e a sister clade among current vent and seep deep-sea Ampharetinae.

34 efficient transfer of organic matter to the deep sea and better preservation of organic matter due t

35 s for understanding fisheries impacts in the deep sea and how these impacts may propagate across dept

36 trate that, despite its remote location, the deep sea and its fragile habitats are already being expo

37 The ability to colonize the deep sea and the periphery of new vent systems may be fa

38 Deep-sea anglerfishes are relatively abundant and divers

39 as a distinctive mode of reproduction among deep-sea anglerfishes.

40 e described from material taken in different deep-sea areas of the Atlantic and Pacific oceans.

41 suspend 78.7 Mt/yr of sediment from shelf to deep-sea areas of the northern South China Sea.

42 This corroborates the deep sea as a major sink for microplastics and the prese

43 nd nutrients, thereby supporting life in the deep sea, as well as soaking up CO2 from the atmosphere.

44 protection measures to preserve these unique deep-sea assemblages showing the uncommon co-existence o

45 tease, myroicolsin, which is secreted by the deep sea bacterium Myroides profundi D25, was purified a

46 n-like collagenolytic protease secreted by a deep sea bacterium, shedding light on the degradation me

47 hage integrated at the 3'-end of ssrA in the deep-sea bacterium S. putrefaciens.

48 adually from the Arctic continental shelf to deep-sea basin.

49 metropolitan area, and revealed a hotspot of deep-sea benthic biodiversity of sessile fauna at ca. 40

50 e fast-sinking particles control the pace of deep-sea benthic communities that live a feast-or-famine

51 of the most pristine locations on earth, the deep-sea benthic ecosystems of the archipelago are virtu

52 t of oxygen and carbon isotope variations in deep-sea benthic foraminifera.

53 loor is pivotal to understand its effects on deep-sea benthic habitats.

54 uct the first systematic characterization of deep-sea benthic invertebrate communities of the Galapag

55 This characterization of Galapagos deep-sea benthic invertebrate megafauna across a range o

56 ls and terrestrial plants and extinctions of deep-sea benthic organisms.

57 are known to supply oxygen and nutrients to deep-sea benthos, suggesting that deep-sea biodiversity

58 Climate drivers will alter deep-sea biodiversity and associated ecosystem services,

59 trients to deep-sea benthos, suggesting that deep-sea biodiversity hotspots are also likely to be mic

60 The distribution, drivers and origins of deep-sea biodiversity remain unknown at global scales.

61 ts that may help to explain discrepancies in deep-sea biogeochemical budgets.

62 ransport, transformation, and degradation to deep-sea biogeochemical processes.

63 in facilitating lateral gene transfer in the deep-sea biosphere.

64 iogeochemical climate models, and imply that deep-sea biota may be sensitive to future changes in pro

65 ch exhibits characteristics of slow-growing, deep sea brachiopods.

66 rmine how cetaceans and pinnipeds accomplish deep-sea chases, we deployed animal-borne instruments th

67 develop a quantitative ecosystem model of a deep-sea chemosynthetic ecosystem from the most southerl

68 hemical cycling, seafloor methane stability, deep-sea circulation, and CO2 cycling.

69 oup of the SAR324 Deltaproteobacteria, three deep-sea clades (Deep sea-1/symbiont-like, Deep sea-2/PS

70 onship of Parablepharismea to the uncultured deep-sea class Cariacotrichea on the basis of single-gen

71 ow higher biomass in a warmed world (+3.2%), deep-sea communities experience a substantial decline (-

72 e wider ranges of species in the pelagic and deep-sea compared to coastal areas.

73 Finally, deep-sea conservation efforts should focus primarily on

74 of fossil-bound organic matter in the stony deep-sea coral Desmophyllum dianthus, a tool for reconst

75 Stalagmite, deep-sea coral, and mollusk shell samples yielded compar

76 234)U/(238)U records based on well-preserved deep-sea corals from the low-latitude Atlantic and Pacif

77 imates, from water column profiles of fossil deep-sea corals in a limited area of the western North A

78 radiocarbon data from uranium-thorium-dated deep-sea corals in the Equatorial Atlantic and Drake Pas

79 c delta(13)C records preserved in long-lived deep-sea corals revealed three major plankton regimes co

80 mentation measured with sediment traps or in deep sea cores.

81 Comparisons with deep-sea data from the same region suggest little exchan

82 vidence for seasonally recurring patterns in deep-sea demersal fish abundances over a 7-year period,

83 2,000 m depth (0.4-0.9 nmol/kg above typical deep-sea dFe concentrations) was determined to be hydrot

84 ivity) and proximity to slope habitats drive deep-sea diversity.

85 30-40 mmolC/m(3), and (iii) the mean age of deep-sea DOC is several times the age of deep water with

86 microbes if concentrated, (ii) the modelled deep-sea DOC reaches stable concentrations of 30-40 mmol

87 e (SST) estimates from southwestern Atlantic Deep Sea Drilling Project Site 516 (paleolatitude ~36 de

88 biotic and abiotic resources from within the deep sea (e.g., fisheries, oil-gas extraction, and minin

89 n acidification on the feeding behavior of a deep-sea echinoid, the sea urchin, Strongylocentrotus fr

90 tegies and monitoring based on widely agreed deep-sea ecological variables.

91 can contribute to a broader understanding of deep sea ecology and biogeochemical cycles in hydrotherm

92 traits is a serious impediment to modelling deep-sea ecosystem connectivity; this uncertainty greatl

93 mportant, previously ignored contribution to deep-sea ecosystem functioning and has an important role

94 dentified as crucial features for monitoring deep-sea ecosystem health, while global climate change w

95 ng of hierarchical ecological information on deep-sea ecosystems (i.e., from single species' abundanc

96 ability to preserve both benthic and pelagic deep-sea ecosystems depends upon effective ecosystem-bas

97 The influence of ocean acidification in deep-sea ecosystems is poorly understood but is expected

98 rigin) influences the functioning of benthic deep-sea ecosystems remains completely unknown.

99 s across the sea floor, and demonstrate that deep-sea ecosystems show a biodiversity pattern consiste

100 rtality in the world oceans, particularly in deep-sea ecosystems where nearly all of the prokaryotic

101 portance of bottom-up trophic structuring in deep-sea ecosystems, we hypothesize that a large fractio

102 In benthic deep-sea ecosystems, which represent the largest biome o

103 e sensitivity, biodiversity, and dynamics of deep-sea ecosystems.

104 and viral metagenomes from different benthic deep-sea ecosystems.

105 view of viral taxonomic diversity in benthic deep-sea ecosystems.

106 ortant source of labile organic compounds in deep-sea ecosystems.

107 r its global range and has a unique niche in deep-sea ecosystems.

108 demonstrate their usefulness as sensors in a deep-sea environment.

109 a affect toxicity, and whether adaptation to deep-sea environmental conditions moderates any effects

110 oposed mining of sulfide massive deposits in deep-sea environments and increased use deep-sea tailing

111 ted to environmental sequences obtained from deep-sea environments based on 16S rRNA gene similarity

112 Understanding life history strategies in deep-sea environments is lacking for many species of fis

113 es, where mates are difficult to find, or in deep-sea environments with limited energy sources.

114 ulfides from active and inactive chimneys in deep-sea environments.

115 Here, we identify a set of deep-sea essential ecological variables among five scien

116 analysis indicates a wide consensus amongst deep-sea experts that monitoring should prioritize large

117 Enteropneusta and Pterobranchia, placed the deep-sea family Torquaratoridae within Ptychoderidae, an

118 The same excursions are recorded in fringing deep-sea fans and in carbonate platforms on other paleoc

119 provided evidence of the ingestion of MPs by deep-sea fauna, but knowledge of MPs' fate once ingested

120 ductivity, biodiversity and distributions of deep-sea fauna, thereby compromising key ecosystem servi

121 arding potential ecotoxicological impacts on deep-sea fauna.

122 ation into other novel reproductive modes of deep-sea fauna.

123 We present a reconstruction of deep-sea Fe isotopic compositions from a Pacific Fe-Mn c

124 of pseudotanaid diversity is correlated with deep-sea features, particularly the presence of fracture

125 ption of this unique life history trait in a deep-sea fish and fills in a gap in the larval literatur

126 nal (intra-annual) migratory behaviours in a deep-sea fish assemblage on the West African margin and,

127 Most deep-sea fish have a single visual pigment maximally sen

128 cold-water coral and commercially important deep-sea fish species under present-day (1951-2000) envi

129 biotic and endogenous metabolizing system of deep-sea fish were compared.

130 ylamine- N-oxide, an osmolyte upregulated in deep-sea fish, significantly enhances the stability of t

131 rently considering new legislation to manage deep-sea fisheries, including the introduction of a dept

132 ck skin (reflectance <0.5%) in 16 species of deep-sea fishes across seven distantly related orders.

133 r corals and a shift in suitable habitat for deep-sea fishes of 2.0 degrees -9.9 degrees towards high

134 e abundance of commercial fish species since deep-sea fishing commenced in the 1970s.

135 impacted by the spill have been impacted by deep-sea fishing operations.

136 ss the event and a lack of extinction at the deep sea floor.

137 By examining organisms that live on the deep-sea floor we show that plastic microfibres are inge

138 This first deep-sea FOCE experiment demonstrated the utility of the

139 These Ediacaran deep-sea fossils were preserved during the increasing ox

140 We used a newly developed deep-sea free ocean CO2 enrichment (dp-FOCE) system to e

141 Argoarchaeum at deep-sea gas seeps(10-12) suggests that archaea that are

142 the family Solariellidae, a group of small, deep-sea gastropods.

143 tunity for assessing spatial patterns in the deep-sea, given their low mobility and limited dispersal

144 The deep sea (>200 m depth) encompasses >95% of the world's

145 In much of the deep sea (>200 m water depth), the export of nutrients f

146 sticated than at present to capture the full deep-sea habitat heterogeneity and biodiversity.

147 boldt squid, Dosidicus gigas, in its natural deep-sea habitat.

148 Given increasing anthropogenic threats on deep sea habitats worldwide, this work has implications

149 resentative of the middle and lower slope of deep-sea habitats.

150 Many fisheries in the deep sea have a track record of being unsustainable.

151 of low-molecular weight organic compounds in deep-sea hot springs are compelling owing to implication

152 Our finding of abiogenic formate in deep-sea hot springs has significant implications for mi

153 e recently been taken into assessment of the deep-sea hydrodynamic variability.

154 Deep-sea hydrogenetic ferromanganese crusts are both pot

155 William Brazelton introduces deep sea hydrothermal vents and the unusual life forms t

156 ic and piezophilic bacterium isolated from a deep-sea hydrothermal chimney.

157 However, the virosphere associated with deep-sea hydrothermal ecosystems remains largely unexplo

158 ke are highly expressed in the Guaymas Basin deep-sea hydrothermal plume.

159 ochemical and biogeochemical analysis of the deep-sea hydrothermal vent ecosystems rely on water samp

160 For deep-sea hydrothermal vent tubeworms (Vestimentifera, Si

161 Deep-sea hydrothermal vents are a significant source of

162 Deep-sea hydrothermal vents are a significant source of

163 Deep-sea hydrothermal vents are highly dynamic habitats

164 Deep-sea hydrothermal vents are patchily distributed eco

165 Many invertebrates at deep-sea hydrothermal vents depend upon bacterial symbio

166 d that large chemosynthetic mussels found at deep-sea hydrothermal vents descend from much smaller sp

167 he discovery of chemosynthetic ecosystems at deep-sea hydrothermal vents in 1977 changed our view of

168 ated from environmental samples ranging from deep-sea hydrothermal vents to insect guts, providing a

169 Bathymodiolinae) are globally distributed at deep-sea hydrothermal vents, depend upon chemoautotrophi

170 At deep-sea hydrothermal vents, microbial communities thriv

171 obial populations in the warm subseafloor of deep-sea hydrothermal vents.

172 Thermotogales, an order well represented in deep-sea hydrothermal vents.

173 eeding on xylem and phloem, and surviving in deep-sea hydrothermal vents.

174 ve tailings deposition has severe impacts on deep-sea infaunal communities and these impacts are dete

175 presenting the first global comparison for a deep-sea invertebrate, demonstrate that V. infernalis ha

176 he eye, has not been previously described in deep-sea invertebrates.

177 Mineral prospecting in the deep sea is increasing, promoting concern regarding pote

178 While the deep sea is low in energy, it also can be highly turbule

179 e environments such as Polar Regions and the deep sea is scarce.

180 The deep sea is the world's largest ecosystem, with high lev

181 ents are still poorly understood because the deep sea is undersampled, the molecular tools used to da

182 ibiont found on members of the species-rich, deep-sea lantern shark family Etmopteridae (Figure 1A) b

183 hesize that the vertical swimming ability of deep-sea larvae, before they permanently settle at the b

184 years, inefficiency in carbon export to the deep sea lasted much longer.

185 e is little published information on octopod deep-sea life cycles and distribution.

186 itus) is the principal limiting resource for deep-sea life.

187 The deep sea Madeira Abyssal Plain contains a 43 million yea

188 degrees C) and sulphidic (> 1 mM SigmaH(2)S) deep-sea methane seep ecosystems.

189 distribution and biogeochemical controls in deep-sea methane seep sediment.

190 ed, due to a lack of cultured representative deep-sea methanotrophic prokaryotes.

191 Deep sea mining concerns the extraction of poly-metallic

192 nodules are a marine resource considered for deep sea mining.

193 fundamental to properly assess the impact of deep sea mining.

194 lop sound environmental management plans for deep-sea mining.

195 Deep-sea mussels (Bathymodiolinae) are globally distribu

196 Deep-sea neutrino telescopes instrumented with light det

197 Deep-sea observation efforts that prioritize these varia

198 itation of species within a diverse genus of deep-sea octocorals, Chrysogorgia, for which few classic

199 eport on the first observations of the giant deep-sea octopus Haliphron atlanticus with prey.

200 ennial climate perturbations that purged the deep sea of sequestered carbon dioxide via a "bipolar ve

201 nd poecilosclerid sponges from asphalt-rich, deep-sea oil seeps at Campeche Knolls in the southern Gu

202 gh ocean water as commonly occurred during a deep-sea oil spill or a natural seep, and enables detail

203 lter physical transport of droplets during a deep-sea oil spill with dispersant.

204 ol for pressure sensors for operation in the deep sea or at extreme conditions.

205 n WTS, and their diet was mainly composed of deep-sea organisms.

206 of increased concentrations of osmolytes in deep-sea organisms.

207 Here we analyze a new high-resolution deep-sea oxygen isotope (delta(18)O) record from the Sou

208 egies and predator-prey interactions of many deep-sea pelagic organisms are still unknown.

209 ps integrate the biogeography of coastal and deep-sea, pelagic and benthic environments, and show how

210 Deep-sea piezophile-like Gammaproteobacteria, along with

211 The deep sea plays a critical role in global climate regulat

212 ere, we present the results of novel in situ deep sea plume experiments undertaken on the Tropic seam

213 00 mum) in the 400 m thick Deepwater Horizon deep-sea plume?

214 natural gas into the Gulf of Mexico, forming deep-sea plumes of dispersed oil droplets and dissolved

215 eviously unobserved level of dynamism in the deep sea, potentially mirroring the great migrations so

216 nt open ocean pelagic CaCO(3) production and deep-sea preservation and assess impacts and feedbacks o

217 reveal 18 continental-shelf and 12 offshore deep-sea realms, reflecting the wider ranges of species

218 rol their dispersal and concentration in the deep sea remain largely unknown.

219 ood chains and vertical carbon export to the deep sea remains unknown, but their prevalence in expand

220 The deep sea represents the largest and least explored biome

221 Even though the deep sea represents the largest area in the world, evolu

222 Conducting an expert elicitation (1,155 deep-sea scientists consulted and 112 respondents), our

223 Deep-sea scleractinian coral reefs are protected ecologi

224 The absence of observations of deep-sea scleractinian reefs in the Central and Northeas

225 d Southern Ocean regions through studying 30 deep-sea sediment cores.

226 Hence, identifying the behaviour of deep-sea sediment plumes is important in designing minin

227 interstellar (60)Fe was extracted from five deep-sea sediment samples and accelerator mass spectrome

228 h conclusions drawn from earlier analyses of deep-sea sediment trap and export flux data, which sugge

229 edding light on the degradation mechanism of deep sea sedimentary organic nitrogen.

230 such an impact is causing the degradation of deep-sea sedimentary habitats and an infaunal depauperat

231 A compilation of Cenozoic deep-sea sedimentary phosphorus speciation data provides

232 ifera abundance and stable isotope ratios in deep sea sediments from Ocean Drilling Program site 984

233 ules (manganese nodules) have been formed on deep sea sediments over millions of years and are curren

234 s, as much as four times more than in low OC deep sea sediments.

235 ious independent approaches, we show that in deep-sea sediments an important fraction of viruses, onc

236 res are formed in specific locations such as deep-sea sediments and the permafrost based on demanding

237 Virus decomposition rates in deep-sea sediments are high even at abyssal depths and a

238 utnumber ray-finned fish teeth in Cretaceous deep-sea sediments around the world, there is a dramatic

239 isotope probing to demonstrate that ANME in deep-sea sediments can be catabolically and anabolically

240 habitat characteristics of the mycobiota of deep-sea sediments collected from the Mexican exclusive

241 Overall, we infer that deep-sea sediments experiencing thermogenic hydrocarbon

242 w temperatures was investigated in subarctic deep-sea sediments in the Faroe Shetland Channel (FSC).

243 m metagenomic data derived from hydrothermal deep-sea sediments in the hydrocarbon-rich Guaymas Basin

244 ariations in the burial of organic carbon in deep-sea sediments over the last glacial cycle.

245 Proxy data from deep-sea sediments suggest that the variability of atmos

246 rk dermal scales (ichthyoliths) preserved in deep-sea sediments to study the changes in the pelagic f

247 p ocean, also have potential implication for deep-sea sediments transport.

248 he biogeography of the fungal community from deep-sea sediments, and identifies the geographic and ph

249 2 million barrels of oil that stayed in the deep sea settled on the bottom.

250 s NanoLuc luciferase (Nluc) derived from the deep-sea shrimp Oplophorus gracilirostris.

251 ed small luciferase subunit (NanoLuc) of the deep-sea shrimp Oplophorus gracilirostris.

252 el optimized luciferase originating from the deep-sea shrimp Oplophorus gracilirostris.

253 bioluminescent light organs (photophores) of deep-sea shrimp, an autogenic system in which the organi

254 fishes, otoliths from families Bathylagidae (deep-sea smelts) and Myctophidae (lanternfish) are most

255 ing how climate change can lead to shifts in deep-sea species distributions is critically important i

256 ogical difficulties in assessing toxicity in deep-sea species has promoted interest in developing sha

257 he uncommon co-existence of such a number of deep-sea species in a single habitat.

258 imate change will affect the distribution of deep-sea species including commercially important fishes

259 In contrast, deep-sea species show maximum richness at higher latitud

260 ades, we find that accumulating knowledge of deep-sea species will likely shift the relative richness

261 may be suitable ecotoxicological proxies for deep-sea species, dependent on adaptation to habitats wi

262 In many deep-sea species, it has long been documented that photo

263 distributions and cause local extinction in deep-sea species.

264 dingly scarce natural product derived from a deep-sea sponge.

265 h place of life on earth could have been the deep sea, studies of pressure effects on LLPS as present

266 enomic bins assembled from the metagenome of deep-sea subsurface sediments shows that the metabolism

267 d by increasing anthropogenic impacts to the deep-sea, such as global ocean change and hydrocarbon ex

268 fossil crinoids and modern crinoids from the deep sea suggests that bioactive polycyclic quinones rel

269 , hydrothermal vents, coastal sediments, and deep-sea surface and subsurface sediments.

270 Deep-Sea Tailings Placement (DSTP) from terrestrial mine

271 s in deep-sea environments and increased use deep-sea tailings placement (DSTP) in coastal zones has

272 tion of potential source populations for the deep-sea taxa protected by the closures; and (3) the deg

273 rge because of the presumed low tolerance of deep-sea taxa to environmental change.

274 ecting 101 fish genomes, we found that three deep-sea teleost lineages have independently expanded th

275 The record displays major oscillations in deep-sea temperature and Antarctic ice volume in respons

276 We find that deep-sea temperature and sea level generally decreased t

277 Ice volume (and hence sea level) and deep-sea temperature are key measures of global climate

278 delta(18)O record for global ice volume and deep-sea temperature variations.

279 For deep-sea temperature, only one continuous high-resolutio

280 reconstruction, with associated estimates of deep-sea temperature, which independently validates the

281 ring glacials with more modest reductions in deep-sea temperature.

282 In the deep sea, the sense of time is dependent on geophysical

283 rrestrial sediment and organic carbon to the deep sea through submarine canyons.

284 he bioluminescence-biased but basically dark deep sea to clear mountain streams.

285 ith marine mammals moving nutrients from the deep sea to surface waters, seabirds and anadromous fish

286 With deep-sea trawling currently conducted along most contine

287 edominantly anthropogenic, is transported to deep-sea trenches primarily in carrion, and then incorpo

288 compositions of amphipods and snailfish from deep-sea trenches reveal information on the sources and

289 ed that organisms travelled in discontinuous deep-sea undular vortices consisting of chains of inerti

290 suggests that the chemosensory behavior of a deep-sea urchin may be impaired by ocean acidification.

291 biotic chemistry under extreme conditions in deep-sea vents or hydrothermal surface sites.

292 The brain architecture of shrimp living in deep-sea vents provides clues to how these organisms hav

293 barriers of interconnected micropores within deep-sea vents.

294 and mostly in the early Earth environment of deep-sea volcanoes and DFTR's characteristics suggest th

295 en prevailing on early Earth and present day deep-sea volcanoes, the potential for the F420/F420H2 pa

296 e accumulation rate of organic carbon in the deep sea was consistently higher (50%) during glacial ma

297 volved under ambient or high pressure in the deep-sea, we detail transition state ensembles that diff

298 conditions, such as those encountered in the deep sea where pressures up to the kbar-level are encoun

299 l clicks pneumatically to detect prey in the deep sea where this long-range sensory channel makes the

300 riving under high-pressure conditions in the deep sea, with pressure of up to 1 kbar, have to cope wi

301 ting significantly to chemical fluxes in the deep sea, yet little is known about the microbial commun